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3+ • Pharmacosiderite KFe4 (AsO4)3(OH)4 6−7H2O c 2001-2005 Data Publishing, version 1

Crystal Data: Cubic. Point Group: 43m. Commonly in good , dominantly cubic, striated diagonally, with minor {111}, {111}, {011}, {122}, to 2 cm. May be granular or earthy. Twinning: Lamellar, visible optically; rarely as twinned tetrahedra.

Physical Properties: : On {001}, good to imperfect. : Uneven. Tenacity: Somewhat sectile. Hardness = 2.5 D(meas.) = 2.797 D(calc.) = 2.90 Weakly piezoelectric and pyroelectric.

Optical Properties: Transparent to translucent. : Olive-, grass-green, emerald-green, honey-, yellowish , dark brown; less commonly hyacinth-, brownish red; in transmitted light, green, yellow, pale brown, biaxially sectored. Luster: Adamantine to greasy. Optical Class: Isotropic; commonly anomalously biaxial (+) or biaxial (–), with weak birefringence, perhaps showing six biaxial sectors. Dispersion: r> vor r

Cell Data: Space Group: P 43m. a = 7.93–7.98 Z = 1

X-ray Powder Pattern: Pednandrea mine, Cornwall, England. (ICDD 34-155). 4.61 (100), 8.0 (90), 2.408 (80), 3.259 (70), 2.822 (65), 1.7844 (65), 1.5959 (60)

Chemistry: (1) (2)

P2O5 1.20 As2O5 37.16 39.88 Fe2O3 37.58 36.95 K2O 4.54 5.45 H2O 18.85 17.72 Total 99.33 100.00

• (1) Cornwall, England; K is exchangeable for H, Ba, Na, etc. (2) KFe4(AsO4)3(OH)4 6.5H2O Occurrence: An oxidation product of -bearing sulfides.

Association: Scorodite, , , arseniosiderite, symplesite, jarosite, “limonite”.

Distribution: Many localities, in small amounts. In England, in Cornwall, from the Carharrack and Tincroft mines and Wheals Gorland and Unity, Gwennap, and a number of other localities; at many mines in Caldbeck Fells, Cumbria. From Vaulry, Haute-Vienne, and at the Cap Garonne mine, near le Pradet, Var, France. In Germany, from Dernbach and Horhausen, Rhineland-Palatinate; at the Clara mine, near Oberwolfach, and elsewhere in the Black Forest; from Schneeberg, Saxony, Germany. From Nova Bana, near Baˇnsk´a Stiavnicaˇ (Schemnitz), Slovakia. In the USA, in the Mammoth mine, Tintic district, Juab Co., Utah; from the Northumberland mine, Nye Co., and as large crystals at the Majuba Hill mine, Antelope district, Pershing Co., Nevada. From Tsumeb, Namibia. At Broken Hill, New South Wales, Australia.

Name: From the Greek for poison, for the arsenic content, and in the composition.

References: (1) Palache, C., H. Berman, and C. Frondel (1951) Dana’s system of mineralogy, (7th edition), v. II, 995–997. (2) Buerger, M.J., W.A. Dollase, and I. Garaycochea-Wittke (1967) The structure and composition of the mineral pharmacosiderite. Zeits. Krist., 125, 92–108. (3) Greis, O., G. Mutter, and W. Eysel (1981) Pulverr¨ontgenographische Untersuchungen an • verschiedenen Pharmakosideriten A[Fe4(OH)4(AsO4)3] (5−7)H2O. Zeits. Krist., 156, 48–49 (in German). (4) Mutter, G., W. Eysel, O. Greis, and K. Schmetzer (1984) chemistry of natural and ion-exchanged pharmacosiderites. Neues Jahrb. Mineral., Monatsh., 183–192. All rights reserved. No part of this publication may be reproduced, stored in a retrieval system or transmitted in any form or by any means, electronic, mechanical, photocopying, recording, or otherwise without the prior written permission of Mineral Data Publishing.